The heat capacities of five mineral samples from the scapolite solid-solution series, Na4Al3Si9O24Cl (marialite) to Ca4Al6Si6O24CO3 (meionite), were measured by the adiabatic method from T=8 K to T=350 K and by the differential scanning calorimetry (d.s.c.) method from T = 300 K to T = 1000 K. The m
Thermodynamic properties of sodalite at temperatures from 15 K to 1000 K
β Scribed by Norikazu Komada; Edgar F. Westrum; Jr.; Bruce S. Hemingway; Mikhail Yu. Zolotov; Yury V. Semenov; Igor L. Khodakovsky; Lawrence M. Anovitz
- Publisher
- Elsevier Science
- Year
- 1995
- Tongue
- English
- Weight
- 521 KB
- Volume
- 27
- Category
- Article
- ISSN
- 0021-9614
No coin nor oath required. For personal study only.
β¦ Synopsis
The heat capacity of sodalite was measured with a computerized adiabatic calorimetric system at temperatures from 15 K to 350 K and with a d.s.c. from 340 K to 1000 K. No anomalies were observed over the entire range except for a peak at T1250 K associated with fusion of NaCl(aq) fluid inclusions. The temperature of the spontaneous freezing of the fluid inclusions was remarkably reproducible, and the metastable liquid phase persisted from T=250 K to 200 K upon cooling. The standard molar entropy for the end-member composition: Na8(Al6Si6O24)Cl2 is 102.0β’R at T=298.15 K. The enthalpy of solution of sodalite was measured in 2PbOβ’B2O3(l) at T=973 K with a Calvet-type calorimeter. The value of DsolHΒ°m(973 K) is (58.9820.71)β’10 3 β’Rβ’K. The calculated standard molar enthalpy and standard molar Gibbs free energy of formation for Na(Al6Si6O24)Cl2 are -(1618.621.9)β’10 3 β’Rβ’K and -(1527.922.0)β’10 3 β’Rβ’K, respectively. 7 1995 Academic Press Limited a A large portion of the work reported here is a part of the dissertation of one of the authors (N.K.) submitted to the H. H. Rackham School of Graduate Studies of the University of Michigan in partial fulfillment of the requirements for the Ph.D. in Chemistry.
π SIMILAR VOLUMES
Osmotic coefficients f of aqueous solutions of 1-n-decanepyridinium chloride, 1-n-dodecanepyridinium chloride, and 1-n-hexadecanepyridinium chloride are estimated at T = 328.15 K from vapor pressure osmometric measurements. Molar integral enthalpies of dilution DdilHm have been measured for aqueous
The heat capacity of manganese monophosphide MnP has been determined by adiabatic shield calorimetry at temperatures from 5 K to 840 K. The heli-to ferromagnetic transition is noted only as a slightly enhanced heat capacity at T f 53 K. A -type heat capacity contribution with maximum at T s 289.5 K
Heat-capacity measurements were made on deerite and on grunerite with an adiabatic calorimetric system from the temperature 10 K to 350 K and by d.s.c. in the super-ambient region. Slight Schottky-like and bell-shaped anomalies appear near T=16 K and 34 K in the deerite heat-capacity curve. The smal
Excess enthalpies, excess heat capacities, densities, and speeds of sound of (ethylbenzene or propylbenzene or 1-methylethylbenzene+cyclohexane) were measured at the temperature 298.15 K. From these measurement, excess volumes, excess isentropic and isothermal compressibilities, and excess isochoric